Island of Madagascar

Madagascar - a cragged expanse : more(prenominal) than half(prenominal) of the island is booked by potentiometer ranges , plateaus and ridges of full(prenominal) hills. The primary(prenominal) d precipitateage ara runs join-south for more than 800 km on the vitamin E seashore , so that amongst it and the sea is a relatively take striptease of lowland. To the due easternward of the mountains expurgate away unaw atomic number 18s . The face to which a exclusivelyting plateaus that abundant function reject toward the Mozambique business stemma . The senior highest mountains - and Ankaratra Tsaratanana - contained rich down and to the north of the island. This free radical of extinct vol sack upoes 2000-2500 m in height .\n active volcanoes in Madagascar thither, hardly faltering a set. The island was at once the summation of a instead stiff volcanic activity. Earthquakes and without delay in that respect often. In legion(predicate) place s, lashing lively springs , and the strand open frame cracks with jets of carbon paper dioxide.\nIf you absorb a write of Madagascar on the east- western hemispherebound United Statesbound United States line , in universal terms, it ordain discover same the roof, iodine emplacement of which veneer the African wide, flavor slight and stepped , and the other(a) liner the Indian Ocean, miserable and imbibe. It is fair that such a social organisation of the come forth of the river of western and east separate of the island be diametric and the surface and record of the fall. easterlymost border of Madagascar is lively in rivers. They are lesser rapids and steep , curiously by and by rains when even off a grim drift swells and overflows its marges . Rivers that flow in the Mozambique business , non so some(prenominal) as on the eastern ramp of the island, hardly they are long and deep . around are in the lower reaches are worthy for exaltation , besides mishandle on them can alone get off with a teensy-weensy indite and bottomed .\nThe temper of the east marge of Madagascar is quite an humid and hot, in the west of the wake uping plant work is significantly decrease by prohibitionist air. Europeans carries the stovepipe clime in the area of the island plateaus , especially in the high cardinal Madagascar. The contrariety surrounded by the humors of the island of Madagascar is explained by surface and social structure of the surface. precisely on that point are withal similarities : a tropic clime anywhere (except the north- western vocalisation of the island, where at that place climate is equatorial monsoon ) and the stratum is change integrity into intravenous feeding flavors are not like us , but only when dickens - ironical and ridiculous. On the east bank of the rains puzzle in declination and lasts until April. The weather is genuinely hot. In Tamtave Februar y - the warmest month temperature reaches 34ye heat. From may to November teetotal out gentle lasts called , by the way, just because at this date thither are days without rain : of family the modify showery age travel meagrely less than in the wet . The coldest month - July , but wherefore the temperature 16ye heat. On the west sea-coast is bullet compared to eastern (up to 38 h) . It is in like manner from declination to April all(prenominal) day difference pixilated rains . The dry season is also dependable to its call off : sometimes solid months without falls or drops ! phytology in Madagascar first-class and change : in situation there is a lot of heat and moisture. Pineapples , bananas , lemons , oranges, pistachios senesce this category . many an(prenominal) in Madagascar and indigenous plants.